For irrotational flow, . Incompressibility gives the Laplace equationThe rigid side walls impose no penetration:and decay in the infinitely deep fluid requires as .
Linearizing the kinematic condition from part (a) about givesThe Unsteady Bernoulli equation, evaluated at the surface and linearized about hydrostatic equilibrium, gives the dynamic conditionThese are the linearized free-surface boundary conditions. Initial values for and specify the transient; below we also record the initially quiescent solution.
Forthe normal derivative at contains and the normal derivative at contains . Both therefore vanish at the side walls.
At , has exactly the same horizontal dependence as the imposed pressure. The dynamic boundary condition is consequently consistent provided has that same horizontal mode. This is the rectangular standing surface-gravity mode selected by the forcing.
Substitution into givesSetThen . Since the fluid occupies , decay as forces . Absorbing into and choosing givesThis is the usual exponential depth dependence of a deep-water gravity wave.
The dynamic condition reduces toDifferentiate and define the natural frequencyThen the surface amplitude obeys the forced harmonic oscillatorFor , its general solution and the corresponding potential amplitude are
The denominators in part (v) vanish when the forcing frequency equals the natural surface gravity wave frequencyAt this value, the initially quiescent resonant solution isBoth contain a term growing linearly in time. This is resonance: the pressure forcing repeatedly supplies energy in phase with the box's standing-wave mode. In the ideal inviscid linear model there is no damping or nonlinear saturation, so its amplitude is unbounded. This is the resonance of a pressure-forced rectangular surface-gravity mode.
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